2012
DOI: 10.1051/swsc/2012009
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The effects of changing solar activity on climate: contributions from palaeoclimatological studies

Abstract: Natural climate change currently acts in concert with human-induced changes in the climate system. To disentangle the natural variability in the climate system and the human-induced effects on the global climate, a critical analysis of climate change in the past may offer a better understanding of the processes that drive the global climate system. In this review paper, we present palaeoclimatological evidence for the past influence of solar variability on Earth's climate, highlighting the effects of solar for… Show more

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Cited by 40 publications
(29 citation statements)
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References 84 publications
(102 reference statements)
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“…Observed oscillations are highly similar to the cyclic signal of changes in total solar irradiance (TSI) with a periodicity of ∼ 11 years (Schwabe cycle) between a sunspot minimum and a sunspot maximum, measured instrumentally in the last 3 decades (Frohlich, 2006;Engels and van Geel, 2012) (Fig. 5).…”
Section: Resultssupporting
confidence: 62%
“…Observed oscillations are highly similar to the cyclic signal of changes in total solar irradiance (TSI) with a periodicity of ∼ 11 years (Schwabe cycle) between a sunspot minimum and a sunspot maximum, measured instrumentally in the last 3 decades (Frohlich, 2006;Engels and van Geel, 2012) (Fig. 5).…”
Section: Resultssupporting
confidence: 62%
“…The so-called "Little Ice Age" in the 17'th century was linked to the Maunder minimum in solar activity by [4]. Many later works have linked climate changes to changes in solar activity (see reviews [5,6]). …”
Section: Introductionmentioning
confidence: 99%
“…a.C. si è verificato un raffreddamento climatico, causato dalla riduzione dell'attività solare, che, rispetto a quanto accade oggi (e a quanto accaduto nelle altre fasi calde dell'Olocene), dovette determinare la persistenza del fronte polare a latitudini più basse anche durante l'estate, con la conseguenza dell'instaurarsi di un clima più ventoso, più freddo e più umido. A livello di durata percentuale nel corso dell'anno, dovette quindi verificarsi nel Mediterraneo una maggior persistenza delle condizioni climatiche invernali e, di conseguenza, una minor durata di quelle estive (Harvey, 1980;O'Brien et al, 1995;Guerrero, 2006: 96-98;Engels, van Geel, 2012;van Geel, Ziegler, 2013: 432-436). Possiamo dunque ipotizzare che in quel periodo il regime dei venti di Bora abbia conosciuto in Adriatico una persistenza superiore rispetto a quanto accade oggi.…”
Section: L'incidenza Del Contesto Ambientaleunclassified